『Abstract
　We studied the dissolution of biotite and chlorite in laboratory systems with flow-through and batch reactors. The initial dissolution of biotite in the near-neutral pH region, under N2(g) atmosphere is highly non-stoichiometric. A slow linear release of iron during a period of weeks indicates a surface-chemical-reaction-controlled mechanism of release for iron. The release of potassium is much faster than that of iron. A parabolic dependence of accumulated release with time suggests a diffusion-controlled mechanism of potassium release. The rates of magnesium, aluminium and silicon release are between those for potassium and iron and approach that of iron with time. There is no significant influence of (bi)carbonate or pH on biotite dissolution rate or stoichiometry in the pH region 7＜pH＜8.5. The release rates of elements from chlorite are close to stoichiometric and similar to the iron release rate from biotite. In closed batch reactors at near-basic pH the composition of test solutions in contact with biotite is apparently controlled by gibbsite (Al), kaolinite (Si) and Fe(III)-(hydr)oxide. We estimated a turn-over time (10¹-10² yr) for molecular oxygen and a time scale (10 months) to develop characteristic Fe(II) concentrations for a granitic groundwater.』

1. Introduction
2. Experiments
　2.1. Mineral characterization and sample preparation
　2.2. Experimental procedure
　　2.2.1. Kinetic experiment
　　2.2.2. Equilibrium experiments
　　　2.2.2.1. Batch experiments
　　　2.2.2.2. Titration experiments
3. Results and discussion
　3.1. Kinetic experiment
　3.2. Equilibrium experiments
4. Implications for groundwater redox chemistry
Acknowledgements
References